Advection and Diffusion Inferred from SST Anomaly Time Series

  • Leonid I. Piterbarg
  • Alexander G. Ostrovskii


In chapter 9 we introduced the background physics for the stochastic model originated by Hasselmann (1976). So far Hasselmann’s theory is the only theory that describes SST nonseasonal variability in the middle latitudes. The advection-diffusion equation (9.42) governs SST anomaly transport and dissipation. Since (9.42) is identical to (6.1) and (7.1), we can use the autoregressive and maximum likelihood estimators developed in chapters 6–8 for extracting SST anomaly advection, diffusion, feedback, and the atmospheric forcing from observations. We will focus on the estimation of the velocity and diffusivity.


Diffusion Estimate Kuroshio Current Subtropical Gyre Kuroshio Extension Ocean Mixed Layer 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

Copyright information

© Springer Science+Business Media Dordrecht 1997

Authors and Affiliations

  • Leonid I. Piterbarg
    • 1
  • Alexander G. Ostrovskii
    • 2
  1. 1.Center for Applied Mathematical SciencesUniversity of Southern CaliforniaLos AngelesUSA
  2. 2.Research Institute for Applied MechanicsKyushu UniversityKasugaJapan

Personalised recommendations